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Contribution of research borehole data to modelling fine-grained turbidite reservoir analogues,Permian Tanqua-Karoo basin-floor fans (South Africa)

机译:研究钻孔数据对模拟细颗粒浊积岩储层类似物的贡献,二叠纪Tanqua-Karoo盆地地扇(南非)

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Outcrop analogue studies can be augmented and constrained by drilling research wells through the same stratigraphic interval.Close-to-outcrop wells help to validate outcrop observations with well log and core data and thus improve the use of such data in actual field developments.Research wells located further away from the outcrops increase the spatial data coverage and can give important insight into regional facies distributions and net:gross changes.In the Tanqua-Karoo Basin (South Africa),seven wells were drilled into fine-grained sand-rich basin-floor fans and interfan mudstones to supplement outcrop data.Three close-to-outcrop wells proved useful in establishing characteristic log responses of the main architectural elements identified from the nearby outcrops.Lithofacies were correcdy identified in more than 80% of cases using an artificial neural network.Borehole images provided detailed information on sedimentary structures,including a wealth of palaeocurrent data from climbing ripples that significantly enhanced the interpretations based only on outcrops.Wells sited away from the outcrops supplied information on lateral thickness and facies trends and intrafan stacking patterns,which helped to define the stratigraphic evolution of the fans.The combined data indicate that deposition was controlled in part by subtle basin-floor topography,and that intrafan lobe switching took place,leading to internal subdivisions that potentially caused effective compartmentalization of the basin-floor fan.
机译:可以通过在相同的地层间隔内钻探研究井来增加和限制露头类比研究,而接近露头的井则有助于通过测井和核心数据验证露头的观测结果,从而改善此类数据在实际油田开发中的使用。位于距露头较远的地方,可以增加空间数据的覆盖范围,并且可以深入了解区域相分布和净值,总值变化。在坦夸-卡鲁盆地(南非),七口井被钻探成细粒富砂盆地。地面扇和扇间泥岩补充露头数据。三个近露头井被证明有助于建立从附近露头中识别出的主要建筑元素的特征测井响应。在超过80%的情况下,使用人工神经网络可以准确地识别出岩相钻孔图像提供了有关沉积物结构的详细信息,包括来自clipi的大量古流数据ng波纹极大地增强了仅基于露头的解释。远离露头的井提供了有关侧向厚度和相貌趋势以及扇内堆积模式的信息,这有助于确定扇的地层演化。综合数据表明沉积受到控制部分是由于微妙的盆底地形,并且发生了扇内瓣转换,从而导致内部细分,潜在地导致了盆底扇的有效分隔。

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